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Distributions of Soil Phosphorus in China's Densely Populated Village Landscapes

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Distributions of Soil Phosphorus in China's Densely Populated Village Landscapes Distributions of soil phosphorus in China’s densely populated village landscapes Linzhang Yang Institute of Soil Science, Chinese Academy of Sciences, Nanjing, 210008, China Abstract Village landscapes, which integrate small-scale agriculture with housing, forestry and other land use practices, cover more than 2×106 km2 across China. And accumulation of excess phosphorous in soils has become an important contributor to eutrophication across China. The aim of this study was to investigate relationships between fine-scale patterns of agricultural management and soil total phosphorus (STP) within China’s village landscapes. The results showed that STP stock across five village regions (0.9×106 km2) was approximately 0.14 Pg (1 Pg=1015 g), with village landscape STP density varying significantly with precipitation and temperature. Outside the Tropical Hilly Region, STP densities also varied significantly with land use, and cover. As expected, the highest STP densities were found in agricultural lands and in areas near buildings, while the lowest were in nonproductive lands and forestry lands. A surprisingly large portion of village STP stock was associated with built structures and disturbed lands surrounding them, which had a significant relationship with population density. Our results demonstrated that local patterns of land management and human residence were associated with substantial differences in STP both within and across China’s village landscapes. Key Words Phosphorus density, village landscape, China. Introduction Phosphorus (P) is highly heterogeneous in spatial distribution, and P inputs are critical in determining whether eutrophication occurs (Vadas et al. 2007). It is therefore critical to understand how P varies in response to climate, land use, and other factors when evaluating the role of terrestrial ecosystem processes in altering the global P cycle. Landscape change is an important part of environmental earth dynamics (Vitousek 1994). Densely populated villages cover approximately 8×106 km2 globally, and in China alone, village landscapes was about 25% of the global village area (Ellis 2004). Changes in land use and land cover within China’s intensively populated village landscapes are dominated by fine-scale landscape changes, preventing the precise measurement of these changes using conventional, coarse-resolution ( ≥30 m), land- use mapping systems (Ellis et al. 2006). For this reason, fine-scale (<1 m) feature-based mapping is an especially useful system for these small changes (Ellis et al. 2000; Ellis et al. 2006). Methods Study area and landscape classfication China’s village landscapes (>150 persons per square kilometer) were first stratified into five biophysically distinct initial regions using a K-means cluster analysis of data for terrain, climate, and soil fertility as illustrated in Table 1(Verburg et al. 1999). Within each region, a single 100 km2 rural landscape site was then selected for detailed field research. Within each site, 12 500×500 m square landscape sample cells (25 ha) were then selected for fine-scale mapping, soil sampling, and other field measurements using a regional cluster analysis of land cover patterns (Ellis 2004). Ecologically-distinct anthropogenic landscape features were mapped across each sample cell based on 1 m resolution IKONOS imagery and orthorectified across each site in 2002 (Ellis et. al., 2006). Landscape features were classified into ecotopes using the four level classification hierarchy: FORM →USE →COVER →GROUP+TYPE, combining simple land use and cover classes (FORM, USE, COVER) with a set of more detailed feature management and vegetation classes (GROUPs) stratified into TYPEs (Ellis et al. 2006; http://ecotope.org/aem/classification). Sampling and Analysis Soil samples were selected using a multi-stage stratified sampling procedure designed to allocate a maximum of about 150 soil sample points within each site among the ecotope classes. First, a maximum of 10 and a minimum of 3 samples were allocated to each ecotope class in direct proportion to their regional areas. A © 2010 19 th World Congress of Soil Science, Soil Solutions for a Changing World 46 1 – 6 August 2010, Brisbane, Australia. Published on DVD. spatially random point location was then chosen within each feature using GIS. Soil core was extracted using an AMS Split Core sampler (AMS, American Falls, Idaho), and the submerged sediments in Yangtze Plain Region were sampled using a coring tube system (Uwitec, Austria). All statistical tests were conducted using SPSS 11.5 (SPSS, Chicago, Illinois, USA). P values < 0.05 were used to test statistical significance in all analyses. One-way analysis of variance (ANOVA) was used to examine the effect of land use, and land cover classes on STP densities. Table 1. Sampled regions and sites (modified from Ellis 2004) Agricultural Annual Main soil types Area Arable Flat Poor Annual Population Mean Region Site (County, Province) (US Soil Taxonomy, (10 3 Land land soils Precipitation density Temperature suborder level) km 2) (%) (%) (%) (mm) (pers km 2) (°C) North China Plain Gaoyi, Hebei Ochrepts, Umbrepts 321 486 51 61 6 645 9 Yangtze Plain Yixing, Jiangsu Fluvents 464 75 44 70 17 1312 16 Sichuan Hilly Jintang, Sichuan Orthents, Psamments 248 198 30 4 5 950 11 Subtropical Hilly Yiyang, Hunan Aqualfs 188 172 18 5 85 1426 14 Tropical Hilly Dianbai, Guangdong Aquults 233 71 20 16 78 1651 20 Results STP densities and stocks Total STP stock (0–30 cm) across the 0.908×106 km2 area of the five regions was approximately 0.144 Pg, and the average STP density was 0.16 kg m–2 (30 cm) (Table 2). The regionally STP density ranged from 0.08±0.04 kg/m 2 in Tropical Hilly to 0.22 kg m–2 both in North China Plain (0.22±0.04 kg/m 2) and in Yangtze Floodplain (0.22±0.19 kg /m 2), which was almost a four fold difference (Table 2). The Tropical Hilly Regions had the lowest STP density because the hydrothermal conditions of high precipitation and temperature can enhance the degree of soil weathering and P loss through surface soil erosion (Neufeldt et al. 2000). In contrast, the higher STP densities of the North China Plain and the Yangtze Plain may be attributed to the large area of arable land with high P fertilizer inputs (Tang et al. 2003). In our study, the annual precipitation (R=0.99, P=0.02) and mean annual temperature (R=0.95, P=0.05) were highly related to STP densities. In the natural land ecosystem, the STP density was highest in the North China Plain, and lowest in the Tropical Hilly, and the distribution and cycle of STP at the regional scale related to climatic, geography (China Agriculture University, 1998), the same rule in our study (except the Yangtze Plain). Table 2. STP density and stock across five regions Region (site) Area Samples Sampled ecotope area ‡ STP STP stock (10 6 km 2) (%) (kg /m2) (Pg) North China Plain (Gaoyi) 0.276 134 94.4 0.22±0.04 0.062±0.011 Yangtze Floodplain (Yixing) 0.086 153 91.8 0.22±0.19 0.019±0.016 Sichuan Hilly (Jintang) 0.084 147 91.0 0.19±0.04 0.016±0.003 Subtropical Hilly (Yiyang) 0.284 152 92.0 0.11±0.03 0.032±0.009 Tropical Hilly (Dianbai) 0.178 149 93.3 0.08±0.04 0.014±0.007 All regions 0.908 735 92.5 0.16 0.144 ‡ Total sampled ecotope area was less than 100%, because ecotope classes with areas ≤ 0.25% of each site were omitted from the sample. Hierarchical scale-effects on STP densities and stocks STP densities varied strongly with land use in every region except Tropical Hilly (Table 3), demonstrating that land use was likely a significant factor controlling STP densities in village landscapes. In all regions, the Constructed (Artificial surfaces and structures) had the highest STP density, because of runoff carrying high levels of P from human and animal waste origin; and decomposing of plant and animal bones releasing high levels of P (China Agricultural University 1998). While, the Forestry USE (0.10 kg m–2) had the lowest average STP density, confirming Grerup et al. ’s (2006) results that total P tended to be higher in the formerly cultivated fields than in the continuously forested land. Variations in STP distribution results could be affected by differences in parent material, soil weathering, human effects, and the relative importance of these factors among regions. STP stock was calculated using STP density and its area. It was therefore not surprising that the largest STP for a given region was related to the extent of the land USE. Each region had a unique dominant land Use and STP stock: North China plain (Irrigated, 78.4%), Yangtze Plain (Paddy, 51.2%), Sichuan Hilly (Rainfed, 49.9%), Subtropical Hilly (Paddy, 37.5%), Tropical Hilly (Forestry, 42.4%) (Table 3). © 2010 19 th World Congress of Soil Science, Soil Solutions for a Changing World 47 1 – 6 August 2010, Brisbane, Australia. Published on DVD. In each region, the distribution of STP density under the level of land COVER was presented in Table 4. Across the five regions, the highest average STP density presented was Sealed COVER (0.23 kg m–2), followed by perennial (0.19 kg m–2) and annual COVER (0.17 kg /m 2), and the lowest STP density was found in Barren COVER (0.07 kg /m 2) (Table 4). But in our results, the Sealed COVER with low vegetation cover had the highest STP density. This is because the sealed COVER (roads, housings) had high soil bulk densities due to human and vehicle’s traffic along with considerable human disturbance and P pollution which coupled contributed to high STP densities. The Annual COVER had the highest STP stock percentage in each region except Tropical Hilly (Perennial COVER had the highest STP stock percentage).
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